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Avalanches
An avalanche is a slide of snow down a slope. It originates in what is called a starting zone, typically high up on a slope, beneath cornices, or in a bowl on a mountainside. The avalanche continues along the avalanche track of snow movement. The avalanche track commonly follows a slope or chute that is treeless and has debris deposited by the avalanche at the bottom of the slope. The track may be just a few feet long, or several hundreds of feet long. The avalanche ends where the snow stops in a runout zone, the site of the largest piles of snow and debris such as trees and rocks.
Snow avalanches may occur as a loose snow slide or as a slab avalanche depending on the slope, recent weather conditions, and characteristics of the snowpack. Loose snow avalanches occur when the snow has little cohesion. The more dangerous slab avalanches occur when a cohesive slab of snow overlies a less cohesive weak layer. In both types, the avalanche begins when a stress is applied that exceeds the strength holding the snow in place. Examples of stresses are the addition of new or windblown snow, a falling snow cornice, the weight of a person on the slope, or explosives used to trigger the avalanche.
Avalanches become a hazard when humans build transportation routes, erect structures, or participate in outdoor recreation in areas prone to avalanches. Avalanches occur throughout the world where snow accumulates on slopes. There are several factors that contribute to avalanches and their impacts, as well as mitigation efforts against avalanches.
Impacts of Avalanches
Avalanches can destroy property, disrupt transportation and communication networks and recreational facilities, and cause human injuries and deaths. These effects occur through the forward force of the moving snow, the crushing weight of snow where it stops, and smothering of people buried in the snow. Recent avalanches caused property damages of $9.1 million in Iceland (1995) and $3 million in Tajikistan (2005). Expensive programs are in place to reduce the impacts of avalanches. Costs for avalanche prevention and mitigation programs in Austria and Switzerland alone for the past 50 years totaled $2.3 billion.
The average annual number of deaths due to avalanches is more than 150 worldwide and is increasing. There are about 100 deaths annually in Europe, 25 in the United States, and 15 in Canada. Avalanches kill a disproportionate number of young people (median age 25–33 years) and men (88 percent). Worldwide, most victims of avalanches are participating in outdoor winter activities, such as climbing, back-country skiing, out-of-bounds skiing, helicat skiing, or snowmobiling. Victims are commonly buried in the avalanche and the primary causes of death are asphyxia and trauma. In Iceland, where many communities have been established along the steep coasts of deep fjords on avalanche-prone terrain, more deaths occur in buildings than outdoors. About 680 people have been killed by avalanches in Iceland since the 12th century.
The deadliest avalanche in U.S. history killed 96 people on two snowbound trains near Stevens Pass, Washington, on March 1, 1910. At least 70 prospectors traveling to the Klondike Gold Fields were killed by an avalanche on the Chilkoot Pass, Alaska, on April 3, 1898.
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